Abstract

Magnetite (MAG) and magnetites substituted with nickel, cobalt and chromium (NF, COF and CRF, respectively) have been prepared over the whole range of composition, Me x Fe 3− x O 4 ( x=0–3, Me=Ni, Co or Cr) using the coprecipitation technique and have been characterized for their chemical composition, crystallinity and surface area. The types of sorption sites present in them were characterized by analysing the water sorption isotherms ultilizing the D'Arcy and Watt equation. Intrinsic dissociation constants, pK ∗ ai and point of zero charge, PZC, were evaluated by analysing the pH-titration curves in acid and alkaline media. A similarity in the trend was observed for the crystallinity, surface area, sorption sites and surface charge characteristics as a function of the composition of the substituted MAGs (i.e. x). The overall behaviour of the substituted MAGs could be grouped into two: mixed oxides having composition with x=0–1 and those in the composition region x=1–3. Those in the composition region x=0–1 were crystalline with a lower surface area, less hydrophilic in nature and have surface charge characteristics lower than that of MAG. Those mixed oxides in the composition region x=1–3 nearly had the opposite characteristics, with increasing value of x. The hydrophilicity of the substituted MAGs decreased in the sequence CRF>NF≫COF, and the acidic nature decreased in the sequence NF>CRF>COF.

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